*work in progress

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Various Features Influencing Convection Initiation on 12 June 2002 during IHOP_2002* Tammy M. Weckwerth Tammy M. Weckwerth (NCAR) WWRP Symposium on Nowcasting and Very Short Range Forecasting, Toulouse, France, 5-9 September 2005 *Work in Progress Hanne V. Murphey Hanne V. Murphey (UCLA) Cyrille Flamant Cyrille Flamant (CNRS) Crystalyne R. Pettet Crystalyne R. Pettet (US NWS) Roger M. Wakimoto Roger M. Wakimoto (NCAR) Sophie Bastin Sophie Bastin (NCAR)

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Various Features Influencing Convection Initiation on 12 June 2002 during IHOP_2002* Tammy M. Weckwerth (NCAR). Hanne V. Murphey (UCLA) Cyrille Flamant (CNRS) Crystalyne R. Pettet (US NWS) Roger M. Wakimoto (NCAR) Sophie Bastin (NCAR). *Work in Progress. - PowerPoint PPT Presentation

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Page 1: *Work in Progress

Various Features Influencing Convection Initiation on

12 June 2002 during IHOP_2002*

Tammy M. WeckwerthTammy M. Weckwerth (NCAR)

WWRP Symposium on Nowcasting and Very Short Range Forecasting, Toulouse, France, 5-9 September 2005

*Work in Progress

Hanne V. MurpheyHanne V. Murphey (UCLA)Cyrille FlamantCyrille Flamant (CNRS)

Crystalyne R. PettetCrystalyne R. Pettet (US NWS) Roger M. WakimotoRoger M. Wakimoto (NCAR)

Sophie BastinSophie Bastin (NCAR)

Page 2: *Work in Progress

GOES 11

Page 3: *Work in Progress

Composite Radar

Page 4: *Work in Progress

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12 June 2002

Are the intersections between the waves and outflow preferred regions for CI?

Why did CI occur here?

Are the rolls a factor in CI?

Does the mesolow play a role in CI?

Page 5: *Work in Progress

2050 UTC

CI 19 km from drop line

Page 6: *Work in Progress

• Incomplete soundings – only up to 6 km AGL (445 mb)• No drops in CI air mass

NE SW

Outflow boundary

Dropsonde Leg 2 – CAPE & CIN

Page 7: *Work in Progress

ELDORA Observations of Waves

• ELDORA fields @ 900 m AGL

• Gravity waves in all fields: λ = 6-8 km• Consistent with P-3, MIPS, GOES-11 and radar

dBZe vr

div vort

Page 8: *Work in Progress

ELDORA and Leandre II Wave Impacts

• ELDORA and Leandre II fields @ 400 m AGL• Periodic signature in q, div and vort: λ=6-8 km

km

Page 9: *Work in Progress

OK Mesonet – 18 UTC – Mesolow Impact

• LLJ feeding region of interest• Dewpoints in the high 60s and low 70s

Freedom

Page 10: *Work in Progress

Wind Direction

Wind Speed Mixing Ratio

Moisture Convergence

Freedom, OK MesonetMesolow Impact

• Local increase in southerly flow, perhaps due to mesolow – not observed further south

• Increase in moisture convergence

Page 11: *Work in Progress

Roll Observations

• ELDORA reflectivity and winds @ 400 m AGL• 1.1 km in situ fields show rolls (λ~3.6 km) SE of TP

w

10 km

Page 12: *Work in Progress

Preliminary results

• Mesolow may have aided in enhancing moisture convergence in CI region.

• Waves sampled by ground-based radar, satellite, in situ P-3, low-level MIPS w, ELDORA. Suggestion of Leandre II mixing ratio modulation caused by waves – may be important for CI.

• Rolls observed near CI location with radar and in-situ P-3 – may be important for CI.*

Page 13: *Work in Progress

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GOES-11 Cloud Tracking

• 1st clouds formed along rolls

• Northern cloud formed near wave/outflow intersection

Page 14: *Work in Progress

Ongoing work

• Closely examine ELDORA and Leandre II measurements near CI location

• Modeling study by Sophie Bastin (presented next)

Page 15: *Work in Progress

Thank you.